VZJ Journal of Natural Resources and Life Sciences Education
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Published online 21 May 2009
Published in Vadose Zone J 8:450-461 (2009)
DOI: 10.2136/vzj2008.0022
© 2009 Soil Science Society of America
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SPECIAL SECTION: UZIG USGS

Transport of Tritium Contamination to the Atmosphere in an Arid Environment

C. A. Garciaa,*, B. J. Andraskia, D. A. Stonestromb, C. A. Cooperc, M. J. Johnsona, R. L. Michelb and S. W. Wheatcraftd

a U.S. Geological Survey, 2730 N. Deer Run Rd., Carson City, NV 89701
b U.S. Geological Survey, 345 Middlefield Rd., Menlo Park, CA 94025
c Desert Research Institute, 2215 Raggio Pkwy., Reno, NV 89512
d Dep. of Geological Sciences, Univ. of Nevada, Reno, NV 89557

* Corresponding author (cgarcia{at}usgs.gov).

Received 4 February 2008.

Soil–plant–atmosphere interactions strongly influence water movement in desert unsaturated zones, but little is known about how such interactions affect atmospheric release of subsurface water-borne contaminants. This 2-yr study, performed at the U.S. Geological Survey's Amargosa Desert Research Site in southern Nevada, quantified the magnitude and spatiotemporal variability of tritium (3H) transport from the shallow unsaturated zone to the atmosphere adjacent to a low-level radioactive waste (LLRW) facility. Tritium fluxes were calculated as the product of 3H concentrations in water vapor and respective evaporation and transpiration water-vapor fluxes. Quarterly measured 3H concentrations in soil water vapor and in leaf water of the dominant creosote-bush [Larrea tridentata (DC.) Coville] were spatially extrapolated and temporally interpolated to develop daily maps of contamination across the 0.76-km2 study area. Maximum plant and root-zone soil concentrations (4200 and 8700 Bq L–1, respectively) were measured 25 m from the LLRW facility boundary. Continuous evaporation was estimated using a Priestley–Taylor model and transpiration was computed as the difference between measured eddy-covariance evapotranspiration and estimated evaporation. The mean evaporation/transpiration ratio was 3:1. Tritium released from the study area ranged from 0.12 to 12 µg d–1 and totaled 1.5 mg (8.2 x 1010 Bq) over 2 yr. Tritium flux variability was driven spatially by proximity to 3H source areas and temporally by changes in 3H concentrations and in the partitioning between evaporation and transpiration. Evapotranspiration removed and limited penetration of precipitation beneath native vegetation and fostered upward movement and release of 3H from below the root zone.

Abbreviations: ADRS, Amargosa Desert Research Site • ET, evapotranspiration • 3H, tritium • 3HHO, tritiated water • LLRW, low-level radioactive waste




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J. R. Nimmo, B. J. Andraski, and R. Munoz-Carpena
UZIG USGS Research: Advances through Interdisciplinary Interaction
Vadose Zone J., May 21, 2009; 8(2): 411 - 413.
[Abstract] [Full Text] [PDF]




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